Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Science 20 September 1963:
Vol. 141. no. 3586, pp. 1175 - 1176
DOI: 10.1126/science.141.3586.1175
Prev | Table of Contents | Next

Articles

Magnetite: Preferred Orientation on the Basal Plane of Partially Reduced Hematite

Rolland O. Keeling Jr. 1 and Deane A. Wick 2

1 Department of Physics
2 Department of Metallurgical Engineering, Michigan College of Mining and Technology, Houghton

Crystallites of two different orientations have been observed in the polycrystalline magnetite layer formed by carbon monoxide reduction on the basal plane of a hematite single crystal. The relative reducibility of hematite and magnetite ores may be related to this double orientation.

To Advertise     Find Products

Science. ISSN 0036-8075 (print), 1095-9203 (online)